Difficulty: Easy
Correct Answer: All the above
Explanation:
Introduction / Context:
Pumping tests and well hydraulics use several standard terms to quantify aquifer response: drawdown (depression head), cone of depression, and radius of influence. A stilling well or observation well is used to monitor groundwater levels under near-still conditions to avoid dynamic fluctuations.
Given Data / Assumptions:
Concept / Approach:
Drawdown equals static water level minus pumping water level. Spatial variation of drawdown creates a characteristic cone-shaped surface known as the cone of depression. Radius of influence is the distance from the well at which drawdown becomes negligible for practical purposes. A stilling/observation well reflects the ambient groundwater level (absent rapid dynamic disturbances).
Step-by-Step Solution:
Identify monitoring: stilling well tracks groundwater level reliably.Define drawdown: s = h_static - h_pumped.Conceptualize the cone of depression around the well.Define radius of influence: distance to near-zero drawdown.
Verification / Alternative check:
Log-log and semi-log analyses (e.g., Theis, Cooper–Jacob) utilize observation well drawdowns to estimate transmissivity and storativity, consistent with these definitions.
Why Other Options Are Wrong:
Each individual statement (A–D) is correct; the most complete choice is “All the above.” Selecting only one omits the integrated description of well hydraulics terms.
Common Pitfalls:
Final Answer:
All the above
Discussion & Comments